A single stone was purchased by Aziz Habibi in Morocco, 2014. The piece was sold to Jarkko Kettunen.
(C. Agee, UNM) Microprobe examination of a polished epoxy mount shows of the silicate fraction: ~85% olivine, ~5% pyroxene, ~5% plagioclase. Accessory apatite and troilite. Metal (kamacite and taenite) make up approximately 15% of this meteorite. Olivine and pyroxene grain size ranges from ~50-300 μm.
(C. Agee and N. Muttik, UNM) EMPA. Olivine Fa10.2±0.1, Fe/Mn=21±1, n=7; low-Ca pyroxene Fs10.0±0.1Wo1.7?0.1, Fe/Mn=13±0, n=9; plagioclase Ab80.4±0.8An14.9±0.4Or4.6±0.5, n=3. Oxygen Isotopes, laser fluorination (K. Ziegler, UNM), analyses on 3 acid-washed aliquots, 1.6, 1.7, 2.1 mg, gave values δ17O=0.898, 1.025, 0.759, δ18O=3.841, 3.932, 3.536, Δ17O=-1.130, -1.051, -1.108 (linearized, all permil).
Primitive Achondrite (Acapulcoite), moderately weathered.
22.5 g including microprobe mount on deposit UNM, Jarkko Kettunen holds the main mass.
Single stone with dark brown, weathered fusion crust, broken surface reveals dark, very fine, shiny, grains.
Jarkko Kettunen Meteorite Collection © 2019